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首页> 外文期刊>Marine ecology progress series >Re-oligotrophication trajectories of macrophyte assemblages in Mediterranean coastal lagoons based on 17-year time-series
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Re-oligotrophication trajectories of macrophyte assemblages in Mediterranean coastal lagoons based on 17-year time-series

机译:基于17年时间序列的地中海沿岸泻湖大型植物群落的再营养化轨迹

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Since the mid-20th century, Mediterranean lagoons have been affected by eutrophication, leading to significant changes in primary producers. In the early 2000s, management actions have been implemented to reduce nutrient inputs with the aim to achieve a good ecological status as requested by the EU water framework directive. As a result of these actions, a sharp decline in nutrient loads has been recorded in several lagoons leading to an oligotrophication of the water column. The analyses of a long-term data set (1998-2015) of 21 polyhaline and euhaline lagoons with contrasting trophic status allowed us to infer a general scheme for the changes in macrophyte assemblages during the oligotrophication process. Placing hypertrophic and oligotrophic conditions end to end, we inferred that the general pattern for the re-oligotrophication trajectory in Mediterranean coastal lagoons is described by the following sequence, with regime shifts between each state: (1) bare non-vegetated sediments, phytoplankton-dominated state; (2) opportunistic macroalgae; (3) seagrass and perennial macroalgae dominated state. However, we did not observe the latter regime shift for the most eutrophicated lagoons, which, so far, remained stuck in the opportunistic macroalgae state. So far, the shift from dominance of opportunistic macroalgae to a system dominated by seagrasses was only observed in a single lagoon where seagrasses had never completely disappeared, which possibly relates to resilience. More generally, the conditions favoring regime shifts from opportunistic macroalgae to seagrasses are still poorly understood. In conclusion, we describe a generic pattern for re-oligotrophication of Mediterranean coastal lagoons, although a full recovery from highly eutrophied to oligotrophic conditions may require more than a decade and may include conditions that remain so far poorly recognized.
机译:自20世纪中叶以来,地中海泻湖受到富营养化的影响,导致初级生产者发生了重大变化。在2000年代初期,已采取管理措施以减少营养物的投入,以达到欧盟水框架指令要求的良好生态状态。由于这些作用,在几个泻湖中记录到养分含量急剧下降,导致水柱富营养化。对21个多卤水和真盐泻湖的长期数据集(具有营养状态的对比)的分析,使我们能够推断出营养富营养化过程中大型植物群落变化的一般方案。放置肥厚性和贫营养性条件的首尾相接,我们推断地中海沿海泻湖中重新富营养化轨迹的一般模式由以下顺序描述,每个州之间的政权转移:(1)裸露的非植被沉积物,浮游植物-统治状态(2)机会性大型藻类; (3)海草和多年生大型藻类为主。但是,我们并未观察到富营养化程度最高的泻湖的后一种政权转移,到目前为止,泻湖仍处于机会主义的巨藻状态。到目前为止,只有在单个泻湖中观察到从机会性大型藻类的控制向以海草为主的系统的转变,在该泻湖中海草从未完全消失,这可能与复原力有关。更普遍地讲,关于从政权巨藻向海草转移的有利条件仍然知之甚少。总而言之,我们描述了地中海沿海泻湖再富营养化的一般模式,尽管要从高度富营养化到贫营养状态的完全恢复可能需要十年以上的时间,并且可能还包括迄今人们认识不到的条件。

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